Uranium has an atomic number of 92 which means there are 92 protons and 92 electrons in the atomic structure. U-238 has 146 neutrons in the nucleus, but the number of neutrons can vary from 141 to 146. Because uranium is radioactive, it is constantly emitting particles and changing into other elements. Uranium has a well-established radioactive decay series. U-238 and U-235 (which has 143 neutrons) are the most common isotopes of uranium. Uranium naturally contains all three isotopes (U-238, U-235 and U-234), and it rarely varies more than 0.01% from the average composition shown in the table below without our intervention.

White 111 Retro Gymnastics NIKE Men Jordan White s Shoes White Air 3 White To produce fuel-grade uranium, the uranium has to be processed to produce uranium dioxide and to enrich or concentrate the U-235 in the fuel pellets. During this processing, depleted uranium (DU), enriched in U-238 and depleted in U-235, is produced. DU and enriched uranium have numerous civilian and military uses. Since U-235 is the most radioactive isotope of uranium, the removal of it to makes DU the least radioactive phase of uranium, but it still has heavy metal toxicity issues.

Despite any processing, enriched, depleted or natural uranium all behave the same chemically. Uranium ore oxidizes to uranium oxy-hydroxides when exposed to the air and/or water.

U-235, when bombarded by neutrons, fissions or splits into two smaller nuclei and releases energy and starts nuclear chain reaction. Because of the energy released, U-235 is efficient for power generation and the only isotope of uranium that can sustain these reactions. For electrical power plants, this reaction is controlled so that it will not produce too many neutrons or heat and become explosive. Go to The Basics of Nuclear Reactions to find out more about nuclear reactions.

Because uranium decays by emitting alpha particles at a constant rate (half-life = time it takes for half of the material to decay to another substance), uranium minerals are very useful for dating rocks and determining the age of the earth.